From a geotechnical perspective, bedding is a discontinuity in a rock mass.
Sedimentology is concerned, in part, with the origin of bedding. There is
much to be gained by a melding of the two disciplines in the underground co
al-mining sector. Bedding controls the strength uf rock; units in coal meas
ures by defining beams that may or may not span openings. Voussoir beam the
ory can be used to explain how massive sandstone/conglomerate units can spa
n longwall panels and what thickness of roof beam is required to span a coa
l mine roadway. Bedding also controls the way in which stresses are distrib
uted about coal mine openings. By utilizing transverse isotropic elastic pr
operties. the effect, of bedding can be readily implemented in continuum nu
merical codes. Geologists logging core need to discriminate between bedding
as a textural element in the rock and bedding as a geotechnical discontinu
ity. Geotechnical engineers need to explicitly consider bedding when formul
ating their design models. (C) 2001 Elsevier Science B.V. All rights reserv
ed.